Physical Geography 101
Global Radiation Balance
Incoming Radiation
Main source of energy for Earth's surface
Radiation received on one hemisphere only.
ultraviolet radiation:
visible radiation:
infrared radiation:
Outgoing Radiation
Radiation from Earth to space
~1/3 all radiation is reflected into space.
Visible, IR and UV radiation are absorbed.
Reemitted as infrared radiation on night/day sides of sphere.
3 dips in outgoing radiation curve.
___________ and __________ absorb wavelengths of IR, blocking it from going into space.
Radiation Balance
Global Radiation Balance: incoming radiation equals outgoing radiation.
Changes in amounts of incoming vs. outgoing radiation have dramatic effects on global climate.
Insolation
Insolation = Incoming Solar Radiation
Amount of insolation received is primarily controlled by:
Exposure Time
Daily variation:
Seasonal Variation:
Meteorological Variation:
Angle of Incoming Radiation
Daily Variation:
Seasonal Variation:
Latitude Variation:
Sun's rays strike the Earth at an angle.